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用戶:Richard923888/DC15工作區/工程/地球水資源分佈

維基百科，自由的百科全書
A graphical distribution of the locations of water on Earth
Visualisation of the distribution (by volume) of water on Earth. Each tiny cube (such as the one representing biological water) corresponds to approximately 1,000 km³ of water, with a mass of about 1 trillion tonnes (200,000 times that of the Great Pyramid of Giza or five times that of Lake Kariba, arguably the heaviest man-made object). Comprising 1 million tiny cubes, the entire cube would measure about 1,102 km on each side.[1]

The water distribution on earth shows that most water in the Earth's atmosphere and crust comes from the world ocean's saline seawater, while freshwater accounts for only 2.5% of the total. Because the oceans that cover roughly 71% of the area of the Earth reflect blue light, the Earth appears blue from space, and is often referred to as the blue planet and the Pale Blue Dot. An estimated 1.5 to 11 times the amount of water in the oceans may be found hundreds of miles deep within the Earth's interior, although not in liquid form.

The oceanic crust is young, thin and dense, with none of the rocks within it dating from any older than the breakup of Pangaea. Because water is much denser than any gas, this means that water will flow into the "depressions" formed as a result of the high density of oceanic crust. (On a planet like Venus, with no water, the depressions appear to form a vast plain above which rise plateaux). Since the low density rocks of the continental crust contain large quantities of easily eroded salts of the alkali and alkaline earth metals, salt has, over billions of years, accumulated in the oceans as a result of evaporation returning the fresh water to land as rain and snow.

As a result, the vast bulk of the water on Earth is regarded as saline or salt water, with an average salinity of 35‰ (or 3.5%, roughly equivalent to 34 grams of salts in 1 kg of seawater), though this varies slightly according to the amount of runoff received from surrounding land. In all, water from oceans and marginal seas, saline groundwater and water from saline closed lakes amount to over 97% of the water on Earth, though no closed lake stores a globally significant amount of water. Saline groundwater is seldom considered except when evaluating water quality in arid regions.

The remainder of the Earth's water constitutes the planet's fresh water resource. Typically, fresh water is defined as water with a salinity of less than 1 percent that of the oceans - i.e. below around 0.35‰. Water with a salinity between this level and 1‰ is typically referred to as marginal water because it is marginal for many uses by humans and animals. The ratio of salt water to fresh water on Earth is around 40 to 1.

The planet's fresh water is also very unevenly distributed. Although in warm periods such as the Mesozoic and Paleogene when there were no glaciers anywhere on the planet all fresh water was found in rivers and streams, today most fresh water exists in the form of ice, snow, groundwater and soil moisture, with only 0.3% in liquid form on the surface. Of the liquid surface fresh water, 87% is contained in lakes, 11% in swamps, and only 2% in rivers. Small quantities of water also exist in the atmosphere and in living beings. Of these sources, only river water is generally valuable.

Most lakes are in very inhospitable regions such as the glacial lakes of Canada, Lake Baikal in Russia, Lake Khövsgöl in Mongolia, and the African Great Lakes. The North American Great Lakes, which contain 21% of the world's fresh water by volume,[2][3][4] are the exception. They are located in a hospitable region, which is heavily populated. The Great Lakes Basin is home to 33 million people.[5] The Canadian cities of Toronto, Hamilton, Ontario, St. Catharines, Niagara, Oshawa, Windsor, and Barrie, and the United States cities of Duluth, Milwaukee, Chicago, Gary, Detroit, Cleveland, Buffalo, and Rochester, are all located on shores of the Great Lakes.

Although the total volume of groundwater is known to be much greater than that of river runoff, a large proportion of this groundwater is saline and should therefore be classified with the saline water above. There is also a lot of fossil groundwater in arid regions that has never been renewed for thousands of years; this must not be seen as renewable water.

However, fresh groundwater is of great value, especially in arid countries such as India. Its distribution is broadly similar to that of surface river water, but it is easier to store in hot and dry climates because groundwater storages are much more shielded from evaporation than are dams. In countries such as Yemen, groundwater from erratic rainfall during the rainy season is the major source of irrigation water.

Because groundwater recharge is much more difficult to accurately measure than surface runoff, groundwater is not generally used in areas where even fairly limited levels of surface water are available. Even today, estimates of total groundwater recharge vary greatly for the same region depending on what source is used, and cases where fossil groundwater is exploited beyond the recharge rate (including the Ogallala Aquifer[6]) are very frequent and almost always not seriously considered when they were first developed.

鹽水和淡水的分佈

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The total volume of water on Earth is estimated at 1.386 billion km³ (333 million cubic miles), with 97.5% being salt water and 2.5% being fresh water. Of the fresh water, only 0.3% is in liquid form on the surface.[7][8][9] In addition, the lower mantle of inner earth may hold as much as 5 times more water than all surface water combined (all oceans, all lakes, all rivers).[10]

水源 每平方公里水量（立方米） 總水量% 鹽水% 淡水% 液面淡水%
海洋 1,338,000,000（321,000,000） 96.5 99.0
太平洋 669,880,000（160,710,000） 48.3 49.6
大西洋 310,410,900（74,471,500） 22.4 23.0
印度洋 264,000,000（63,000,000） 19.0 19.5
南部海洋 71,800,000（17,200,000） 5.18 5.31
北冰洋 18,750,000（4,500,000） 1.35 1.39
冰及雪 24,364,000（5,845,000） 1.76 69.6
冰川 24,064,000（5,773,000） 1.74 68.7
南極冰蓋 21,600,000（5,200,000） 1.56 61.7
格陵蘭冰蓋 2,340,000（560,000） 0.17 6.68
北極島嶼 83,500（20,000） 0.006 0.24
山脈 40,600（9,700） 0.003 0.12
地面冰和永久凍土 300,000（72,000） 0.022 0.86
地下水 23,400,000（5,600,000） 1.69
地下鹽水 12,870,000（3,090,000） 0.93 0.95
地下淡水 10,530,000（2,530,000） 0.76 30.1
土壤濕度 16,500（4,000） 0.0012 0.047
湖 176,400（42,300） 0.013
鹽湖 85,400（20,500） 0.0062 0.0063
裏海 78,200（18,800） 0.0056 0.0058
其他鹽湖 7,200（1,700） 0.00052 0.00053
淡水湖 91,000（22,000） 0.0066 0.26 87.0
非洲大湖 30,070（7,210） 0.0022 0.086 28.8
貝加爾湖 23,615（5,666） 0.0017 0.067 22.6
北美大湖 22,115（5,306） 0.0016 0.063 21.1
其他淡水湖泊 15,200（3,600） 0.0011 0.043 14.5
大氣層 12,900（3,100） 0.00093 0.037
沼澤 11,470（2,750） 0.00083 0.033 11.0
河流 2,120（510） 0.00015 0.0061 2.03
生物水 1,120（270） 0.000081 0.0032

河水分佈

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The total volume of water in rivers is estimated at 2,120 km³ (510 cubic miles), or 2% of the surface fresh water on Earth.[7] Rivers and basins are often compared not according to their static volume, but to their flow of water, or surface runoff. The distribution of river runoff across the Earth's surface is very uneven.

大陸或地區 河流徑流（km³/年） 佔世界總數的百分比
北美洲 7,800 17.9
南美洲 12,000 27.6
歐洲 2,900 6.7
中東和北非 140 0.3
撒哈拉以南非洲地區 4,000 9.2
亞洲（不包括中東） 13,300 30.6
澳大利亞 440 1.0
大洋洲 6,500 14.9

There can be huge variations within these regions. For example, as much as a quarter of Australia's limited renewable fresh water supply is found in almost uninhabited Cape York Peninsula.[11] Also, even in well-watered continents, there are areas that are extremely short of water, such as Texas in North America, whose renewable water supply totals only 26 km³/year in an area of 695,622 km², or South Africa, with only 44 km³/year in 1,221,037 km².[11] The areas of greatest concentration of renewable water are:

世界海洋的面積，體積和深度

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水體 面積 （106 km2） 體積 （106 km3） 平均深度 （m）
大西洋 82.4 323.6 3,926
太平洋 165.2 707.6 4,282
印度洋 73.4 291.0 3,963
所有海洋 361 1,370 3,796

水可用性的變化

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Variability of water availability is important both for the functioning of aquatic species and also for the availability of water for human use: water that is only available in a few wet years must not be considered renewable. Because most global runoff comes from areas of very low climatic variability, the total global runoff is generally of low variability.

Indeed, even in most arid zones, there tends to be few problems with variability of runoff because most usable sources of water come from high mountain regions which provide highly reliable glacier melt as the chief source of water, which also comes in the summer peak period of high demand for water. This historically aided the development of many of the great civilizations of ancient history, and even today allows for agriculture in such productive areas as the San Joaquin Valley.

However, in Australia and Southern Africa, the story is different. Here, runoff variability is much higher than in other continental regions of the world with similar climates.[12] Typically temperate (Köppen climate classification C) and arid (Köppen climate classification B) climate rivers in Australia and Southern Africa have as much as three times the coefficient of variation of runoff of those in other continental regions.[13] The reason for this is that, whereas all other continents have had their soils largely shaped by Quaternary glaciation and mountain building, soils of Australia and Southern Africa have been largely unaltered since at least the early Cretaceous and generally since the previous ice age in the Carboniferous. Consequently, available nutrient levels in Australian and Southern African soils tend to be orders of magnitude lower than those of similar climates in other continents, and native flora compensate for this through much higher rooting densities (e.g. proteoid roots) to absorb minimal phosphorus and other nutrients. Because these roots absorb so much water, runoff in typical Australian and Southern African rivers does not occur until about 300 mm (12 inches) or more of rainfall has occurred. In other continents, runoff will occur after quite light rainfall due to the low rooting densities.

氣候類型 （柯本[14]） 年平均降雨量 Typical runoff ratio
for Australia and Southern Africa 		Typical runoff ratio
for rest of the world
BWh 250 mm (10 inches) 1 percent (2.5 mm) 10 percent (25 mm)
BSh (on Mediterranean fringe) 350 mm (14 inches) 3 percent (12 mm) 20 percent (80 mm)
Csa 500 mm (20 inches) 5 percent (25 mm) 35 percent (175 mm)
Caf 900 mm (36 inches) 15 percent (150 mm) 45 percent (400 mm)
Cb 1100 mm (43 inches) 25 percent (275 mm) 70 percent (770 mm)

The consequence of this is that many rivers in Australia and Southern Africa (as compared to extremely few in other continents) are theoretically impossible to regulate because rates of evaporation from dams mean a storage sufficiently large to theoretically regulate the river to a given level would actually allow very little draft to be used. Examples of such rivers include those in the Lake Eyre Basin. Even for other Australian rivers, a storage three times as large is needed to provide a third the supply of a comparable climate in southeastern North America or southern China. It also affects aquatic life, favouring strongly those species able to reproduce rapidly after high floods so that some will survive the next drought.

Tropical (Köppen climate classification A) climate rivers in Australia and Southern Africa do not, in contrast, have markedly lower runoff ratios than those of similar climates in other regions of the world. Although soils in tropical Australia and southern Africa are even poorer than those of the arid and temperate parts of these continents, vegetation can use organic phosphorus or phosphate dissolved in rainwater as a source of the nutrient. In cooler and drier climates these two related sources tend to be virtually useless, which is why such specialised means are needed to extract the most minimal phosphorus.

There are other isolated areas of high runoff variability, though these are basically due to erratic rainfall rather than different hydrology. These include:[13]

地幔中的水

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It is estimated an additional 1.5 to eleven times the amount of water in the oceans is contained in the Earth's interior,[15] and some scientists have hypothesized that the water in the mantle is part of a "whole-Earth water cycle".[16] The water in the mantle is dissolved in various minerals near the transition zone between Earth's upper and lower mantle. At temperatures of 1,100 °C（2,010 °F） and extreme pressures found deep underground, water breaks down into hydroxyls and oxygen.[17] The existence of water was experimentally predicted in 2002,[18] and direct evidence of the water was found in 2014 based on tests on a sample of ringwoodite.[19] Further evidence for large quantities of water in the mantle was found in observations of melting in the transition zone from the USArray project.[20] Liquid water is not present within the ringwoodite, rather the components of water (hydrogen and oxygen) are held within as hydroxide ions.[19]

相關條目

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參考文獻

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  1. ^ USGS - Earth's water distribution
  2. ^ Great Lakes – U.S. EPA. Epa.gov. 2006-06-28 [2011-02-19]. 
  3. ^ LUHNA Chapter 6: Historical Landcover Changes in the Great Lakes Region. Biology.usgs.gov. 2003-11-20 [2011-02-19]. （原始內容存檔於2012-01-11）. 
  4. ^ Ghassemi, Fereidoun. Inter-basin water transfer. Cambridge, Cambridge University Press. 2007. ISBN 0-521-86969-2. 
  5. ^ https://www.ec.gc.ca/grandslacs-greatlakes/default.asp?lang=En&n=B4E65F6F-1
  6. ^ Reisner, Marc; Cadillac Desert: The American West and its Disappearing Water; pp. 438-442. ISBN 0-14-017824-4
  7. ^ 7.0 7.1 Where is Earth's water?, United States Geological Survey.
  8. ^ Eakins, B.W. and G.F. Sharman, Volumes of the World's Oceans from ETOPO1, NOAA National Geophysical Data Center, Boulder, CO, 2010.
  9. ^ Water in Crisis: Chapter 2, Peter H. Gleick, Oxford University Press, 1993.
  10. ^ Harder, Ben. Inner Earth May Hold More Water Than the Seas. National Geographic. [14 November 2013]. 
  11. ^ 11.0 11.1 Brown, J. A. H.; Australia’s surface water resources. ISBN 978-0-644-02617-8.
  12. ^ McMahon, T.A. and Finlayson, B.L.; Global Runoff: Continental Comparisons of Annual Flows and Peak Discharges. ISBN 3-923381-27-1.
  13. ^ 13.0 13.1 Peel, Murray C.; McMahon, Thomas A. & Finlayson, Brian L. Continental differences in the variability of annual runoff: update and reassessment. Journal of Hydrology. 2004, 295 (1–4): 185–197. doi:10.1016/j.jhydrol.2004.03.004. 
  14. ^ This section uses a slightly modified version of the Köppen system found in The Times Atlas of the World, 7th edition. ISBN 0-7230-0265-7
  15. ^ Crocket, Christopher. Quest to trace origin of Earth’s water is ‘a complete mess’. Science News. 5 September 2015 [1 October 2015]. 
  16. ^ Melissa Davey. Earth may have underground 'ocean' three times that on surface. The Guardian. 12 Jun 2014 [13 Mar 2015]. 
  17. ^ Earth found hiding huge reservoirs of water 400 miles below...but not water as we know it : SCIENCE : Tech Times. Tech Times. 16 June 1015 [13 October 2015]. 
  18. ^ Ben Harder. Inner Earth May Hold More Water Than the Seas. National Geographic. 7 Mar 2002 [13 Mar 2015]. 
  19. ^ 19.0 19.1 Becky Oskin. Rare Diamond Confirms That Earth's Mantle Holds an Ocean's Worth of Water. Scientific American. 12 Mar 2014 [13 Mar 2015]. 
  20. ^ HENRY FOUNTAIN. The Earth’s Hidden Ocean. New York Times. 6 Jun 2014 [13 Mar 2015]. 

[[Category:水和環境]]

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